Solution of the Inverse Problem of Subsurface Electric Exploration for Horizontally Stratified Medium

Figure 3

The example of additional information 𝑔(𝜔,𝜆) given with the error 𝑃=20% (𝜔∈[𝜔₀/50,𝜔₀/10], 𝜆=5⋅10⁻¹); the exact values of real and imaginary parts of 𝑔(𝜔,𝜆) are shown by the smooth line.